45 downwards because (j on the average increases with height; but this conclusion does not follow from (18.3) when the dependency of Kc upon ~o is taken into consideration. s 2 ERTELl and PRIESTLEY and SWINBANK have shown that the upward eddy flux of sensible heat must be larger than indicated by (18.3), because this formula does not account for the fact that rising eddies are systematically warmer than sinking eddies because of the effect of buoyancy. The reader is referred to the reviews by SUTTON [22], [23] and PRIESTLEY and SHEP PARD [15) for further details concerning eddy-flux of heat and turbulent diffusion. 19. RICHARDSON'S criterion. The right-hand side of (15.10) represents the rate of production of eddy energy. The last term represents energy loss by dissipation; in order that the eddy energy shall be maintained, it is therefore necessary that P div V" - (! V" v" . grad. v > O.

45 downwards because (j on the average increases with height; but this conclusion does not follow from (18.3) when the dependency of Kc upon ~o is taken into consideration. s 2 ERTELl and PRIESTLEY and SWINBANK have shown that the upward eddy flux of sensible heat must be larger than indicated by (18.3), because this formula does not account for the fact that rising eddies are systematically warmer than sinking eddies because of the effect of buoyancy. The reader is referred to the reviews by SUTTON [22], [23] and PRIESTLEY and SHEP PARD [15) for further details concerning eddy-flux of heat and turbulent diffusion. 19. RICHARDSON'S criterion. The right-hand side of (15.10) represents the rate of production of eddy energy. The last term represents energy loss by dissipation; in order that the eddy energy shall be maintained, it is therefore necessary that P div V" - (! V" v" . grad. v > O.

7 Fig. 3. Photographie de la lueur nocturne it I'horizon, obtenue it bord d'une fusee Aerobee it 184 km d'altitude Ie ler (l.

TO APPLIED GEOPHYSICS STANIS LAY MARE~, et al. Faculty of Science, Charles University, Prague SPRINGER-SCIENCE+BUSINESS MEDIA, B. V. Library of Congress Cataloging in Publication Data Mares, Stanislav Introduction to applied geophysics Translation of Uvod do uzite geofyziky Bibliography: p. Includes index. 1. Geophysics. 2. Prospecting-Geophysical methods. I. Title QC802. A1M3713 1984 551 84-4753 ISBN 978-90-481-8374-6 ISBN 978-94-015-7684-0 (eBook) DOI 10. 1007/978-94-015-7684-0 AII Rights Reserved © 1984 by Stanislav Mard et al. Originally published by Kluwer Academic Publishers in 1984 Softcover reprint ofthe hardcover lst edition 1984 No part of the material protected by this copyright notice may be reproduced or utilized in any form or by any means, electronic or mechanical including photocopying, recording or by any information storage and retrieval system, without written permission from the copyright owner CONTENTS XI INTRODUCTION LIST OF PRINCIPAL SYMBOLS AND UNITS USED XIII CHAPTER I. GRAVIMETRIC METHODS (S. Hrach) I. I. Physical principles of gravimetric methods- Volume gravitational potential I 1. 2. Gravity field of the Earth 3 1. 3. Anomalies of gravitational acceleration-Gravity anomalies 9 1. 3. 1. Faye anomaly-Free-air anomaly 9 1. 3. 2. Bouguer anomalies 10 1. 3. 3. Isostatic anomaly 14 1. 3. 4. Geological significance of anomalies 17 1. 4. Rock densities 19 1. 4. 1. Natural rock densities 20 1. 4. 2. Rock density determination 22 1. 4. 3. Determination of density characteristics 25 25 1. 5. Gravity observations 26 1. 5. 1. Instruments for absolute gravity observations 1. 5. 2.

Everyday Applied Geophysics 2: Electromagnetics and Magnetics covers the physical methods permitting the environmental exploration of the sub-surface in 1, 2, 3 or 4 dimensions (the latter for time-lapse in terms of physical environmental state and geometry). The book specifically addresses the feasible methods that are accessible and affordable to all users, providing a simple apparatus of electronic diagrams and free, Internet open-source software links for data interpretation. - Proposes a practical, accessible and affordable applied geophysics resource for sub-surface environmental exploration - Explains the topic's application to groundwater, raw material and resources, agriculture, buried pollutions and archaeology